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首页> 外文期刊>Ocean Dynamics >Modeling the impact of wind and waves on suspended particulate matter fluxes in the East Frisian Wadden Sea (southern North Sea)
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Modeling the impact of wind and waves on suspended particulate matter fluxes in the East Frisian Wadden Sea (southern North Sea)

机译:模拟风和波浪对东弗里斯兰省瓦登海(北海南部)中悬浮颗粒物通量的影响

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摘要

Suspended particulate matter (SPM) fluxes and dynamics are investigated in the East Frisian Wadden Sea using a coupled modeling system based on a hy-drodynamical model [the General Estuarine Transport Model (GETM)], a third-generation wave model [Simulating Waves Nearshore (SWAN)], and a SPM module attached to GETM. Sedimentological observations document that, over longer time periods, finer sediment fractions disappear from the Wadden Sea Region. In order to understand this phenomenon, a series of numerical scenarios were formulated to discriminate possible influences such as tidal currents, wind-enhanced currents, and wind-generated surface waves. Starting with a simple tidal forcing, the considered scenarios are designed to increase the realism step by step to include moderate and strong winds and waves and, finally, to encompass the full effects of one of the strongest storm surges affecting the region in the last hundred years (Storm Britta in November 2006). The results presented here indicate that moderate weather conditions with wind speeds up to 7.5 m/s and small waves lead to a net import of SPM into the East Frisian Wadden Sea. Waves play only a negligible role during thesernconditions. However, for stronger wind conditions with speeds above 13 m/s, wind-generated surface waves have a significant impact on SPM dynamics. Under storm conditions, the numerical results demonstrate that sediments are eroded in front of the barrier islands by enhanced wave action and are transported into the back-barrier basins by the currents. Furthermore, sediment erosion due to waves is significantly enhanced on the tidal flats. Finally, fine sediments are flushed out of the tidal basins due to the combined effect of strong erosion by wind-generated waves and a longer residence time in the water column because of their smaller settling velocities compared to coarser sediments.
机译:使用基于水动力模型[通用河口运输模型(GETM)],第三代波浪模型[近海模拟波浪]的耦合建模系统,研究了东弗里斯兰沃登海的悬浮颗粒物(SPM)通量和动力学。 (SWAN)],以及连接到GETM的SPM模块。沉积学观察表明,在较长的时期内,瓦登海地区消失了更细的沉积物部分。为了理解这种现象,制定了一系列数值方案以区分可能的影响,例如潮汐流,风增强流和风产生的表面波。从简单的潮汐强迫开始,考虑的场景旨在逐步增加真实感,以包括中度和强风和浪潮,最后涵盖最近一百年来影响该地区的最强烈风暴潮之一的全部影响。年(Storm Britta在2006年11月)。此处显示的结果表明,适度的天气条件(风速高达7.5 m / s和小浪)导致SPM净进口到东弗里西亚瓦登海。在现代条件下,波浪只起着微不足道的作用。但是,对于速度高于13 m / s的强风条件,由风产生的表面波对SPM动力学有重大影响。在暴风雨条件下,数值结果表明,沉积物通过增强的波作用而在屏障岛的前面被侵蚀,并被洋流输送到后屏障盆地。此外,在潮滩上由于波浪引起的沉积物侵蚀显着增强。最后,由于与较粗糙的沉积物相比,沉降速度较小,因此,由于风浪强烈侵蚀和较长的在水柱中停留时间的综合作用,精细的沉积物被冲出了潮汐盆地。

著录项

  • 来源
    《Ocean Dynamics》 |2009年第2期|239-262|共24页
  • 作者单位

    Institute for Chemistry and Biology of the Sea (ICBM), Department of Physical Oceanography (Theory), Carl von Ossietzky University Oldenburg, Carl-von-Ossietzky-Str. 9-11, 26111 Oldenburg, Germany;

    Institute for Chemistry and Biology of the Sea (ICBM), Department of Physical Oceanography (Theory), Carl von Ossietzky University Oldenburg, Carl-von-Ossietzky-Str. 9-11, 26111 Oldenburg, Germany;

    Institute of Physics, Department of Marine Physics, Carl von Ossietzky University Oldenburg, Carl-von-Ossietzky-Str. 9-11, 26111 Oldenburg, Germany;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    suspended particulate matter fluxes; wadden sea; tidal flat; surface gravity waves; storm surges; numerical modeling;

    机译:悬浮颗粒物通量;瓦登海潮滩;表面重力波;风暴潮;数值模拟;

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